Aquatic Sciences

, 81:60 | Cite as

Extreme rates and diel variability of planktonic respiration in a shallow sub-arctic lake

  • Matthew J. BogardEmail author
  • Sarah Ellen Johnston
  • Mark. M. Dornblaser
  • Robert G. M. Spencer
  • Robert G. Striegl
  • David E. Butman
Research Article


Planktonic community respiration (CR) is a major component of aquatic biogeochemical cycling and food web energetics. Accurate, direct characterizations of short-term patterns and drivers of plankton CR are needed to understand aquatic biogeochemical processes and food web functioning. Recent work indicates CR may be commonly underestimated, and may undergo considerable diel changes that are missed using standard methodological approaches. To explore these possibilities, we applied an immediate, in situ, dark incubation approach at ~ 3 h intervals over 2.5 diel cycles in a shallow, productive, sub-arctic lake in interior Alaska, USA. Rates of CR varied 17-fold, strongly coupled to diel oscillations in water temperature. A weak inverse relationship to ~ 3 mg L−1 diel changes in dissolved organic carbon concentrations suggests CR partially modulated the standing stock of organic matter over short timescales. Average rates of CR were ~ 6 to 100-fold greater than published, conventional CR measurements, but comparable to existing free-water estimates of ecosystem respiration for nearby Alaskan lakes. Overall, this study places new weight on the importance of CR in whole-ecosystem biogeochemical transformations by supporting recent suggestions that planktonic CR may be commonly underestimated.


Respiration Plankton Metabolism Community Food web Lake Diel 



We thank Jim Webster (Webster’s Flying Service) for transport to and from Canvasback Lake. This project was supported by funding provided to MJB from the Fonds de recherche du Québec–Nature et technologies (FRQNT) and the U.S. Permafrost Association (USPA); to RGS, DEB, and RGMS from National Aeronautics and Space Agency, NASA-ABoVE Project 14-14TE-0012 (awards NNH16AC03I and NNX15AU14A); to DEB from the University of Washington and the U.S. Geological Survey Land Resources Mission Area; and to RGS and MMD from the U.S. Geological Survey Land Resources and Water Mission Areas. We also thank two anonymous reviewers for providing helpful suggestions that improved our manuscript.

Supplementary material

27_2019_657_MOESM1_ESM.docx (427 kb)
Supplementary material 1 (DOCX 426 kb)


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Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  1. 1.School of Environmental and Forest SciencesUniversity of WashingtonSeattleUSA
  2. 2.Florida State UniversityTallahasseeUSA
  3. 3.United States Geological SurveyBoulderUSA
  4. 4.School of Engineering and Environmental SciencesUniversity of WashingtonSeattleUSA
  5. 5.Department of Biological SciencesUniversity of LethbridgeLethbridgeCanada

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